The disclosed invention relates to novel crystalline compositions which may be obtained by doping the alpha (α) form of AlPO4 ceramics, which find use as piezoelectric materials, stable supports for catalysts, biotechnology uses, and the like.

Patent
   7101820
Priority
Mar 06 2002
Filed
May 26 2004
Issued
Sep 05 2006
Expiry
Mar 06 2022

TERM.DISCL.
Assg.orig
Entity
Large
11
3
EXPIRED
1. A doped, single phase, cristobalite AlPO4 composition that exhibits a cubic structure, space group F-43m, with a ˜7.2 Angstroms at a temperature of less than about 270° C. in the absence of transformation from α-phase to β-phase, wherein the dopant is selected from one or both of a silica dopant, and a dopant having a cation with an atomic radius of about 1 angstrom that fits stably within the interstices of the cristobalite structure.
2. A composition according to claim 1 wherein the cubic structure is maintained up to at least 1000° C.
3. A composition according to claim 1 which is at a temperature in the range of from room temperature to about 250° C.
4. A composition according to claim 1 wherein the cation is potassium.
5. A composition according to claim 1 wherein the cation is copper.
6. A composition according to claim 1 wherein the cation is calcium.
7. A composition according to claim 6 which contains excess silica in the molar ratio of calcium to silica.
8. A composition according to claim 1 in the form of a piezoelectrical material, a support in catalysis, a support in biotechnology, a ceramic filler or a ceramic coating.

This application is a continuation of U.S. Ser. No. 10/092,115, filed Mar. 6, 2002, now U.S. Pat. No. 6,749,769, which is incorporated in its entirety as a part hereof for all purposes.

This invention relates to novel crystalline compositions obtained by doping the alpha (α) form of aluminum phosphate ceramics.

The cristobalite phase of aluminum phosphate (AlPO4) ceramic exists in two modifications, the low temperature cristobalite (denoted as, low cristobalite, or α-form) and the high temperature cristobalite (high cristobalite, or β-form). The two modifications are separated by a reversible phase transformation that occurs at about 270° C. The phase transformation results in abrupt volume and structural changes and discontinuous thermal expansion, which are not conducive to technological applications. Structures of the α- and β-phases have been reported by various researchers including Wright and Leadbetter (Phil. Mag. 31, 1391, 1975). AlPO4 is isomorphous with silica and exists with silica in various forms including the α-cristobalite form, with phase transformations at similar temperatures. The structure of the alpha form of AlPO4 is tetragonal, a=b=5.03 Angstroms and c=7.00 Angstroms with space group C2221. The structure of the α-AlPO4 phase is similar to corresponding silica structures with Al and P atoms alternately replacing the silicon atoms. (Mooney, Acta Cryst. 9, 728, 1956) The structure of β-AlPO4 shows a cubic structure, space group F-43m, with a ˜7.2 Angstroms.

It is well known in the glass ceramics field that high temperature forms of silica can be formed at relatively low temperatures by stabilizing the ceramic matrix with dopants. The silica counterpart of the aluminum phosphate materials described above (tetragonal α-cristobalite) undergoes a displacement phase transition to the cubic high temperature β-phase at about 300° C. Various reports regarding the stabilization of cristobalite phases of silica ceramics by various methods have been issued. U.S. Pat. No. 5,096,857, M. A. Saltzberg, et al., J. Amer. Ceram. Soc. 1992, 75, 89, and P. L. Gai, et al., J. Solid State Chemistry, 1993, 106, 35, all describe chemically stabilized solution-derived silica β-cristobalite of the type CaxAlySi1-x-yO2 and its compositions. R. D. Shannon, et al., Phys. and Chem. Miner. 1992, 19, 157, reported compositions in the BPO4/AlPO4/SiO2 system (BAPOS), with compositions up to 75% AlPO4, 75% SiO2 and 50–60% BPO4. A relatively high amount (approximately 15%) BPO4, was used in these studies. The authors reported the presence of secondary amorphous phases (i.e., the materials were not single phase), and suggested that stabilization could be achieved using only framework ions (i.e., no ions in the interstices).

M. Rokita, et al., Pr. Kom. Nauk. Ceram. Pol. Akad. Nauk 1997, 54, 161 describe the synthesis of solid-solutions of SiO2—AlPO4. A single dopant, 20–75% mole % SiO2, was used. The structures and compositions of the solid solution with this single dopant (SiO2) were not determined because the solid solution formed multiphasic systems. Also, a relatively large mole percent (20–75 mole %) of the dopant SiO2 is used in this work. M. Handke, et al., Vib. Spectr, 1999, 19(2) 419–423 show spectroscopic data from these compounds and demonstrate that multiphasic systems are formed.

Stable ceramic materials are required for a number of end-uses, including use as piezoelectrical materials (i.e., structured materials which produce electric polarization when mechanical stress is applied), as stable supports in catalysis and biotechnology, as ceramic fillers with low dielectric constants in electronic application and as ceramic coatings for reactor materials.

In view of the foregoing, it is advantageous to develop a stable ceramic material that is single phasic through a wide range of temperatures.

The present invention relates to a stabilized AlPO4 composition comprising CaO, SiO2 and AlPO4 at a ratio of greater than 0 to less than about 4 mole percent CaO, greater than 0 to less than about 10 mole percent SiO2, greater than about 86 to less than about 100 mole percent AlPO4. The composition more preferably comprises CaO, SiO2 and AlPO4 at a mole percent ratio of greater than 0 to less than about 3 CaO, greater than 0 to less than about 6 SiO2, greater than about 91 to less than about 100 AlPO4. The composition most preferably comprises CaO, SiO2 and AlPO4 at a mole percent ratio of about 2.3 CaO, about 5.7 SiO2, about 92 AlPO4.

The synthesis involves the following steps: preparation of a slurry or sol containing the dopants, gentle drying of the slurry to drive off water and to produce amorphous precursors, and calcination to crystallize the desired phase. These synthesis procedures described below yield powders which are single phase.

The present invention also provides a method for making these compositions, comprising the steps of: admixing an acidic solution of AlPO4 to stoichiometrically appropriate solutions of SiO2 (ammonium stabilized silica sol from DuPont Ludox AS-40) and a calcium oxide source (such as calcium nitrate hydrate) wherein the mole percent ratios are greater than about 86 to less than about 100 AlPO4, greater than 0 to less than about 10 SiO2, greater than 0 to less than about 4 calcium nitrate; and the pH was adjusted to about 2.5. Calcium nitrate is an example of a convenient and economical source of CaO. The admixture is transferred to a continuous stir tank with NH4OH solution to produce a slurry with a pH of about 9. The slurry is gently heated (˜70° C.) to dehydrate and form a precipitate. The precipitates are then heated and calcined at different temperatures and X-ray diffraction measurements were performed. Subsequently, electron microscopy analyses were carried out.

Another embodiment of this invention is an AlPO4 composition that has a cubic structure, space group F-43m, with a ˜7.2 Angstroms at a temperature of less than about 270° C., particularly a temperature in the range of from room temperature (approximately 25° C.) to about 250° C. Previously known aluminum phosphate ceramics did not have the cubic structure except after having undergone a phase change at a temperature of about 270° C. or more.

FIG. 1A is an x-ray powder diffraction scan image of pure, unstabilized α-phase AlPO4.

FIG. 1B is an x-ray powder diffraction scan image of stabilized low temperature (room temperature) β-phase AlPO4, (hereafter referred to as stabilized AlPO4 phase/composition).

FIG. 2A is a scanning electron microscopy (SEM) image of pure, unstabilized α-phase AlPO4.

FIG. 2B is an SEM image of stabilized (β-phase) AlPO4.

FIG. 3A is a high resolution transmission electron microscopy (HREM) image demonstrating the twin, stacking defects in unstabilized α-phase AlPO4.

FIG. 3B is an electron diffraction photograph corresponding to FIG. 3A, showing streaks due to the defects in unstabilized α-phase AlPO4.

FIG. 3C is an x-ray composition analysis, by energy dispersive x-ray spectroscopy (EDX) showing the presence of Al and P in the oxide shown in FIGS. 3A and 3B.

FIG. 4A is an HREM of stabilized AlPO4 (2.3 CaO:5.7 SiO2:92AlPO4), showing no defects.

FIG. 4B is an electron diffraction pattern corresponding to FIG. 4A in (110) orientation.

FIG. 4C is an atomic structure image corresponding to FIG. 4A confirming the absence of defects at the atomic level in the sample.

FIG. 4D is an x-ray compositional (chemical) analysis (EDX) showing the presence of Al, P, Si and Ca in the 2.3 CaO:5.7 SiO2:92 AlPO4 sample used in FIG. 4A.

FIG. 5 is an x-ray powder diffraction pattern of the material made in Comparative Example B (2.5 SiO2:97.5 AlPO4)

FIG. 6A is an x-ray powder diffraction pattern of the material made in Comparative Example C (3 CaO:97 AlPO4).

FIG. 6B is an x-ray compositional (microchemical) analysis (EDX) showing the presence of Al, P and Ca (3 CaO:97 AlPO4).

FIG. 7A is an environmental-HREM (EHREM) photograph showing the α-phase AlPO4 with stacking defects at room temperature.

FIG. 7B is an EHREM photograph showing the relatively defect-free β-phase AlPO4 after the α-form in FIG. 7A is heated in-situ to ˜270° C.

The present invention describes novel compositions of stabilized AlPO4, a room temperature (approximately 25° C.) AlPO4-based ceramic containing small amounts of dopants and prepared by a wet chemical method, which essentially exhibits structural characteristics of the high temperature β-phase without undergoing phase transformations. The structural integrity of these novel single phase ceramics is maintained up to at least 1000° C.

Composition Range

The invention is directed to compositions consisting essentially by mole % of at least about 85%–97% AlPO4, about 3%–10% SiO2 and about 0.3%–5% CaO, in which the composition ratio of CaO/SiO2 is at least about 0.1 to 0.5. The most preferred composition of the single phasic stabilized AlPO4 compound is about 2.3CaO to about 5.7SiO2 to about 92AlPO4.

In the molar range disclosed above, the crystalline compositions of the present invention form the stabilized AlPO4 at room temperature and have structural properties of the high temperature β-phase. These crystalline compositions contain excess silica in the molar ratio of CaO to silica (i.e. contain non-equimolar ratios of CaO to silica). It has been found that this excess silica provides an important advantage in forming single phasic stabilized AlPO4. In the range described above, and at the ratios away from the preferred composition of CaO:SiO2:AlPO4 of about 1 to about 2.5 to about 40, small quantities of secondary phases can be present in these cases with the predominantly stabilized AlPO4 phase without generally changing the properties of the compositions of this invention. Compositions containing ratios other than in the range or ratios described above will form quantities of mixed phases (including a mixture of α- and β-), a result which is not desirable.

Ionic Sizes

Previous work has been done on certain transition metals, alkali and alkaline earth oxide dopants in silica cristobalite phases (Gai, et al., J. Solid State Chem. 106, 35, 1993). Although they may form acceptably small amounts of secondary phases, potassium and copper represent alternatives to calcium as dopants in the stabilization of a high temperature AlPO4 phase.

Calcium is the preferred dopant. It is possible that stabilization is achieved by incorporating Ca ions in the interstices in the cristobalite framework of AlPO4 to prevent the phase transformation. The Ca ions may be charge-compensated by the substitution of Si ions in the AlPO4 framework consistent with the compositional analyses shown herein (FIG. 4D). This mechanism is similar to the silica analogs described by various workers (e.g. A. J. Perrota et al, J. Amer. Ceram. Soc. 72,441(1989) and Gai et al, J. Solid State Chem. 106,35(1993)). The type of the monovalent, divalent or trivalent cation dopants residing in intersticies is likely determined by the size of the ions (i.e. whether these ions will fit stably in the interstices of the cristobalite structure). Ca has an ionic radius of 1.0 Angstroms (R. D. Shannon Acta Cryst. A32, 751, 1976). K and Cu have comparable ionic radii making K and Cu acceptable substitutes for Ca.

Microstructure and Chemical Composition Analyses

Electron Microscopy (EM) Procedures

To understand the microstructure, morphology and chemical composition of the ceramics, a combination of high resolution transmission EM (HREM) with atomic resolution, high resolution low voltage scanning EM (LVSEM) and scanning transmission electron microscopy (STEM) were used. These are described below.

High precision chemical compositional analyses were carried out by electron stimulated energy dispersive X-ray compositional spectroscopy (EDX), to provide high spatial resolution on the (sub) nanometer scale. Chemical composition from localized regions of the ceramic particles follows below. The analyses were carried out using a commercial Vacuum-Generators field emission-gun HB501-STEM and the data were confirmed by using advanced Philips CM200 field emission gun HREM/STEM instrument. Additionally, atomic structural investigations at different temperatures were performed using a modified Philips CM30 environmental-HREM (EHREM) fitted with a sample-heating stage (ref: P. L. Gai, DuPont: published in Advanced Materials, Vol. 10, p. 1259, 1998), and a Philips CM20 HREM All the EMs were equipped with X-ray spectrometers to analyze chemical compositions.

For compositional studies, analyses were recorded from many dozens of crystals in the sample using an electron nanoprobe. For quantitative chemical microanalysis, a ratio method was used and is given by: C(a)/C(b)=constant factor (I (a))/I (b), where C(a) and C(b) are concentrations of the elements a and b, and I(a) and I(b) are the background subtracted peak intensities of (a) and (b) in the X-ray spectrum, using the procedures described by Cliff, G. and Lorimer G. W., J. Microscopy, vol 103, p. 203, 1975. The analyses were calibrated using a standard of single-phase silica and aluminum phosphate compounds.

Complementary experiments on microstructure, morphology and microchemistry of the new ceramic compositions were also performed using a Hitachi high resolution S5000 LVSEM (ref: E. D. Boyes, DuPont: published in Adv. Materials, Vol. 10, p. 1277, 1998). Microstructures and surface topography of the ceramic samples were recorded.

Description of Crystalline Structures

In the present invention, the structure of the stabilized (room/low temperature) composition of AlPO4 with dopants of CaO and silica, is isomorphous with the high temperature β-AlPO4 phase, showing a cubic structure with a ˜7.2 angstroms, by electron and X-ray diffraction.

Potential uses for the stable ceramic materials made by this invention include, but are not limited to, piezoelectric materials, stable supports for catalysis and biotechnology, as ceramic fillers with low dielectric constants in electronic applications, and as ceramic coatings for reactor materials.

As used herein, the term “stabilized” means room or low temperature ceramics containing small amounts of dopants, exhibiting high temperature ceramic phase properties without undergoing phase transformations. When “stabilized” is used with “composition” or “single phasic”, its meaning is extended to include long range order, better sintering properties and higher stability in the presence of molten glass.

As used herein, “phase transformation” refers to the transformation from a low temperature α-phase to a high temperature β-phase.

To prepare a 92 mole % AlPO4 solution, 112.18 g AlPO4 was mixed in 900 mL water and adjusted pH to 2.5 with concentrated HNO3. In a separate beaker, 3.42 g Ludox AS40 (40% SiO2 solution) was mixed with 20 mL of water and pH adjusted to 2.5 with concentrated HNO3 to prepare a 5.7 mole % SiO2 solution. To prepare a 2.3 mole % Ca(NO3)2 solution, 1.28 g Ca(NO3)2 was mixed into 20 mL of water and pH adjusted to 2.5 with concentrated HNO3. Both the SiO2 and Ca(NO3)2 solutions were added to the aluminum phosphate solution, and transferred to a 3 L flask with heating at 70° C.

A solution of 38 mL concentrated NH4OH and water was made for a total volume of 1 L. After transfer to a dropping funnel, this solution was added drop-wise to the previously prepared AlPO4 solution to produce a slurry having a pH of 9. The mixed solutions were stirred overnight at 70° C. The material subsequently formed was filtered and heated in furnace at 500° C. for 6 hours. The material was then calcined at different temperatures and tested by x-ray diffraction. Subsequently Electron Microscopy was Performed on the samples.

Microchemical analyses (FIG. 4D) and STEM of this material show the presence of Si and Ca in the structure and the defect-free material suggests framework substitution of Si with divalent cations in interstitial positions (consistent with charge compensating mechanism described by Buerger (1954)) inhibiting the phase inversion. The defect-free stabilized composition is a cubic structure as illustrated by FIGS. 4A, 4B and 4C. The morphology of the stabilized composition has grains with interconnectivity as illustrated by FIG. 2B.

α-AlPO4 was analyzed by X-ray diffraction, TEM, electron diffraction, SEM, and EDX according to the methods described above. As shown in FIGS. 2A, 3A, 3B and 3C, the morphology of standard α-phase of AlPO4 is different from that of the stabilized material made in Example 1. The structure is tetragonal. The phase has twin-like stacking defect structures, and it undergoes phase transformation.

A composition of 2.5 mole percent SiO2:97.5 mole percent AlPO4 was made using the procedure described in Example 1, except that Ca(NO3)2 was not added. No stabilized composition was noted (see FIG. 5), and the structure appeared very similar to that of the α-phase as shown in FIG. 1A.

A composition of 3 mole percent CaO: 97 mole percent AlPO4 was made using the procedure described in Example 1, except that SiO2 was not used. Both x-ray powder diffraction (FIG. 6A) and EDX (FIG. 6B) showed the presence of Al, P and Ca in the oxide, and the structure still appeared very similar to that of the α-phase as shown in FIG. 1A.

A sample of standard α-cristobalite was placed on the heating stage of the EHREM. As shown in FIG. 7A, there existed stacking defects as would be expected at room temperature. The sample was then heated to about 270° C., when the sample transitioned to the β-phase. The stacking defects disappeared as shown in FIG. 7B. This confirms the results shown in FIG. 4 for the stabilized composition.

Gai, Pratibha Laxman

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